摘要
1984年冬季在金塘水道南岸水域获取了4个测站历时15～30d的近底层流资料。通过一系列统计特征分析及最大熵谱结构分析,对近底层流的潮振动特性及低频流结构有了一定认识。对底摩擦层流动垂向变化,海底地形对底流的影响及低频流的产生机制等问题作了初步探讨。
Based on the bottom current data from four stations along the southern side of the Jintang Channel where observation lasted 15~30 days in winter of 1984,statistical characteristical analyses and the maximum-entropy spectrum analyses are made in this paper and a certain knowledge has been gained on the near bottom tidal fluctuations as well as the low-frequency flow structure of the area concerned.Preliminary studies on the vertical variation of flow in the bottom frictional layer,the effect of bed topography on the bottom flow and the dynamical mechanism of the low-frequency near bottom flow are also presented.
出处
《海洋通报》
CAS
CSCD
北大核心
1989年第4期27-35,6,共10页
Marine Science Bulletin
